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Soil/properties, 4-17 adsorption exchange capacity

Soils and vadose zone information, including soil characteristics (type, holding capacity, temperature, biological activity, and engineering properties), soil chemical characteristics (solubility, ion specification, adsorption, leachability, cation exchange capacity, mineral partition coefficient, and chemical and sorptive properties), and vadose zone characteristics (permeability, variability, porosity, moisture content, chemical characteristics, and extent of contamination)... [Pg.601]

The method of soil suspensions extracts is based on metal desorption/dissolution processes, which primarily depend on the physico-chemical characteristics of the metals, selected soil properties and environmental conditions. Metal adsorption/ desorption and solubility studies are important in the characterization of metal mobility and availability in soils. Metals are, in fact, present within the soil system in different pools and can follow either adsorption and precipitation reactions or desorption and dissolution reactions (Selim and Sparks, 2001). The main factors affecting the relationship between the soluble/mobile and immobile metal pools are soil pH, redox potential, adsorption and exchange capacity, the ionic strength of soil pore water, competing ions and kinetic effects (e.g. contact time) (Evans, 1989 Impelhtteri et al., 2001 McBride, 1994 Sparks, 1995). [Pg.239]

The first natural microporous aluminosilicate, i.e., natural zeolite, was discovered more than 200 years ago, and after long-term practical applications, the intrinsic properties of natural zeolites such as reversible water-adsorption capacity were fully recognized.13 41 By the end of the 19th century, during exploitation of ion-exchange capacity of some soils, it was found that natural zeolites exhibited similar properties some cations in natural zeolites could be ion-exchanged by other metal cations. Meanwhile, natural chabazite could adsorb water, methanol, ethanol, and formic acid vapor, but could hardly adsorb acetone, diethyl ether, or benzene. Soon afterwards, scientists began to realize the importance of such features, and use these materials as adsorbents and desiccants. Later, natural zeolites were also used widely in the field of separation and purification of air. [Pg.2]


See other pages where Soil/properties, 4-17 adsorption exchange capacity is mentioned: [Pg.113]    [Pg.113]    [Pg.186]    [Pg.128]    [Pg.18]    [Pg.250]    [Pg.251]    [Pg.112]    [Pg.116]    [Pg.68]    [Pg.365]    [Pg.368]    [Pg.1667]    [Pg.144]    [Pg.363]    [Pg.195]    [Pg.383]    [Pg.244]    [Pg.312]    [Pg.245]    [Pg.941]    [Pg.4]    [Pg.191]   
See also in sourсe #XX -- [ Pg.141 , Pg.142 ]




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Adsorption properties

Adsorptive capacity

Exchange adsorption

Exchange capacity

Exchange properties

Soil/properties, 4-17 adsorption

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